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Palynology of Knapps Narrows sediment core from the Eastern Shore of Maryland
This dataset has no description
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Dinoflagellate cyst counts from IODP Hole 318-U1356A
This dataset has no description
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Palynological analysis of sediment core GeoB9508-5
This dataset has no description
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(Table T1) Abundance of dinoflagellates and other palynomorphs in ODP Hole 18...
Sediment depth is given in median mbsf. -
(Table T3) Abundance of dinoflagellates and other palynomorphs in ODP Hole 18...
Sediment depth is given in median mbsf. -
(Table T2) Abundance of dinoflagellates and other palynomorphs in ODP Hole 18...
Sediment depth is given in median mbsf. -
(Table T3) Abundance of dinoflagellates and other palynomorphs in Maastrichti...
Sediment depth is given in median mbsf. -
(Table T2) Abundance of dinoflagellates and other palynomorphs in Eocene-Olig...
Sediment depth is given in median mbsf. -
(Table T1) Abundance of dinoflagellates and other palynomorphs in Quaternary ...
Sediment depth is given in median mbsf. Age model adopted from Stickley et al. (2004, doi:10.2973/odp.proc.sr.189.111.2004). -
Dinoflagellate cysts in the Oligocene to Miocene sediments of IODP Site 318-U...
There is growing interest in the scientific community in reconstructing the paleoceanography of the Southern Ocean during the Oligocene-Miocene because these time intervals... -
Dinoflagellate cysts abundances in IODP Site 307-U1318
This dataset has no description
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(Appendix A) Raw counts and stratigraphic range of dinoflagellate cysts and a...
<1 = species recorded outside regular counts. -
(Table T2) Dinoflagellate stratigraphy of ODP Hole 184-1148A
DEPTH, sediment is given in mbsf. Abundance estimate as follows: V = very abundant, A = abundant, C = common, R = rare, P = present, - = not found. -
(Table T1) Abundance of dinoflagellates and other palynomorphs in ODP Hole 18...
Sediment depth is given in mbsf. Age model adopted from Stickley et al. (2004, doi:10.2973/odp.proc.sr.189.111.2004). -
Late Miocene and Pliocene dinoflagellate cysts, acritarchs and terrestrial pa...
The globally warm climate of the early Pliocene gradually cooled from 4 million years ago, synchronous with decreasing atmospheric CO2 concentrations. In contrast,...
